1.
orthotectonic Caledonides
标准构造型加里东褶皱带
2.
A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS
东秦岭与华南加里东褶皱带原地-准原地改造型花岗岩特征
3.
Granites at the middle Variscian period are the largest scale magma activities on the Caledonia foldbelt inthe west Tianshan mountain.
海西中期花岗岩是西天山加里东褶皱带内规模最大的一次岩浆活动。
4.
Characteristics of Caledonian folds in the northern segment of the Yangtze platform:Evidence from unconformity
扬子东南缘北段加里东期的褶皱特征——来自不整合关系的证据
5.
The Folding Time of the Eastern Sichuan Jura-type Fold Belt:Evidence from Unconformity
川东“侏罗山式”褶皱带形成时代:不整合面的证据
6.
THE REGIONAL TECTONIC EVOLUTION OF TARIM BASIN AND ADJACENT FOLD BELTS
塔里木盆地与相邻褶皱带的区域构造演化
7.
Yanshanian Superposed Structural Characteristics of West Margin of Foreland Fold Belt of South Dabashan
燕山期南大巴山前陆褶皱带西缘叠加构造特征
8.
LOWER PALEOZOIC OMISSION ZONE IN JIANGNAN UPLIFT──A SIGN OF CALEDONIAN FORELAND FOLD THRUST BELT
江南隆起上的下古生界缺失带──华南加里东前陆褶冲带的标志
9.
5)Cale-donian fault-fold belt (Hercynian deformation) in the southeast of it ;
5）塔东南中、新元古基底的加里东断褶带（海西改建）；
10.
accumulation zone of thrust fold
逆掩断裂褶皱聚集带
11.
Flow and Deformation Mechanisms of Hornblende Rocks from the Paleoproterozoic Fold Belt in Liaodong Peninsula;
辽东古元古宙褶皱带变质角闪质岩石的流动与变形机制
12.
Structural characteristics and hydrocarbon accumulation of Kuche fold-thrust belts, Talimu Basin
塔里木盆地库车褶皱冲断带的构造特征与油气聚集
13.
These folds are characteristic of a-type fold which are commonly found in ductile shear zones.
这些褶皱的特征表明它们属于a型褶皱，而a型褶皱通常发育在韧性剪切带中。
14.
Some have circled rings around them that are beginning to pucker.
有时乳头周围还会出现带褶皱的圆环。
15.
treated so as to have a permanently wrinkled appearance.
物品加工过的使之有永久皱褶外观的。
16.
THE PRESENT SITUATION OF THE MECHANISM AND THE TYPES IN SUPERPOSED BUCKLE FOLDING
纵弯褶皱叠加机制和类型的研究现状
17.
Qinling fold belt is located at the junction of the North China plate and the Yangtze plate, and its portion in Henan Province is a part of the East Qinling Mountains (EQM).
秦岭褶皱带位于华北板块和扬子板块结合部位，其在河南省内的部分多划为东秦岭。
18.
Antarctica can be divided into 2 big structural units, ie East antarctica shield and West Antarctica Mesozoic Cenozoic fold belt.
南极洲主要可分为东南极地盾及西南极中新生代褶皱带两大构造单元。